Page 104 - General Knowledge
P. 104
GENERAL KNOWLEDGE 2019
There are two important layers in the ionosphere viz. E layer or Kennelly Heavy side layer
that reflects the medium radio waves, thus helping in short distance radio communication
and F layer or Appleton layer that reflects the short radio waves and helps in long distance
radio communication.
The outermost layer of the Earth‘s atmosphere is known as the Exosphere. It is so highly
rarefied a region that its boundary is not clear.
Lithosphere
The lithosphere is an Earth‘s outermost layer, composed of rocks in the crust and upper
mantle that behave as brittle solids.
The rigid lithosphere sits on the top of the asthenosphere, a layer of the mantle in which
rocks are hot and deformable.
The lithosphere is the solid, rocky crust covering the entire planet. This crust is inorganic and
is composed of minerals.
It covers the entire surface of the earth from the top of Mount Everest to the bottom of the
Mariana Trench.
The actual thickness of the lithosphere varies considerably, and can range from roughly 40
km to 280 km.
Earth‘s lithosphere includes the crust and the uppermost mantle, which constitute the hard
and rigid outer layer of the Earth.
The lithosphere is subdivided into tectonic plates.
The lithosphere ends at the point when the minerals in the earth‘s crust begin to
demonstrate viscosity and fluid behaviors.
Rocks
The earth‘s crust is formed of mineral materials called rocks.
The rocks which form the substructure of our lithosphere are grouped into three broad
categories:
Igneous Rocks
Igneous rocks are formed by the solidification of molten magma from the interior of the earth.
About 95% of the earth‘s crust is made of this type of rock. In fact, all other types of rocks
originate from these rocks, and therefore, they are also called primary rocks.
Igneous rocks are of three types.
Characteristics of Igneous Rocks
The igneous rock does not contain layers.
They are without fossils and the upper part of the rock contains joints.
They are formed by volcanic lava.
They are crystalline rocks and impervious rocks.
They are massive and the weathering effect is difficult over them.
They are primary rocks of the crust, hence are also called the primary rocks.
Sedimentary Rocks
These rocks are formed from the sediment deposits on the ocean beds.
They comprise only about 5% of the earth‘s crust, but cover about 75% of the total land
surface.
100 | P a g e shop.ssbcrack.com